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CMI Annual Report 2021

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conditions that favor tropical cyclone genesis (“genesis<br />

probability” in the left panel of Figure 13.1) or the frequency of<br />

pre-TC “seeds” (center panel). However, the combined effect of<br />

variations in genesis probability and seeds yields a sharp<br />

annual cycle that accurately explains hurricane climatology<br />

across both climate models and observations (right panel). The<br />

ability of this theoretical framework to explain the annual<br />

cycle of hurricanes provides an observational test of the<br />

hypothesis, developed in climate simulations, that the<br />

combined role of seeds and genesis probability in the climate<br />

impacts hurricane frequency.<br />

Figure 13.1.<br />

TC seeds and genesis<br />

probability together<br />

explain the annual cycle<br />

of North Atlantic (NA)<br />

hurricane frequency in<br />

observations and climate<br />

models.<br />

Scatter plots of monthly<br />

climatology of NA TC<br />

frequency versus TC genesis<br />

probability index (left<br />

panel), frequency of vortex<br />

seeds (center panel), and the<br />

combination of both (right<br />

panel) from observations<br />

and model historical<br />

simulations from HiRAM,<br />

AM2.5, and AM2.5C360.<br />

All the quantities are<br />

normalized by their annual<br />

total. Dashed lines show<br />

the linear regression, for<br />

which the equation and<br />

the variance explained are<br />

shown on the bottom right<br />

of each panel. The sharp<br />

annual cycle of Atlantic<br />

hurricane frequency is due<br />

to the combined effect of<br />

both seeds and genesis<br />

probability (Yang et al.,<br />

<strong>2021</strong>).<br />

A related study explores the impact of TC seeds on genesis<br />

across a broad suite of climates and climate model<br />

configurations and develops a theory to link seed frequency to<br />

large-scale environmental factors (Hsieh et al., 2022,<br />

submitted). This work has shown that inter-model spread in TC<br />

genesis sensitivity to changing climate is largely driven by<br />

differences in the response of pre-TC synoptic disturbances.<br />

The climatological changes in these disturbances can be<br />

understood in terms of changes to large-scale aspects of the<br />

atmosphere (such as the amount of energy converging in the<br />

atmosphere and the rate at which air ascends). The researchers<br />

are now working to connect observed and modeled changes in<br />

TC frequency to large-scale climatic parameters using first<br />

principles (e.g., conservation of energy, mass and momentum),<br />

in an effort to build a theoretical constraint on tropical cyclone<br />

frequency.<br />

The Vecchi team also explored impacts of uncertainties in<br />

ocean temperature reconstructions and changes in hurricane<br />

monitoring as a way to assess past changes in hurricane<br />

activity. They found that improvements in ocean temperature<br />

53<br />

Carbon Mitigation Initiative Twenty-first Year <strong>Report</strong> <strong>2021</strong>

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